英语翻译The nearshore seafloor environments may be linked to some degree with the stability and behavior of the barrier-island coastline.Recent sonar images of two small areas on the inner shelf have revealed extensive hardgrounds and complex san

英语翻译The nearshore seafloor environments may be linked to some degree with the stability and behavior of the barrier-island coastline.Recent sonar images of two small areas on the inner shelf have revealed extensive hardgrounds and complex san
英语翻译
The nearshore seafloor environments may be linked to some degree with the stability and behavior of the barrier-island coastline.Recent sonar images of two small areas on the inner shelf have revealed extensive hardgrounds and complex sand wave structures indicating active sediment transport.Sonar images collected one year apart suggested some migration of large offshore sand ridges (kilometers in scale) may occur.However,what is missing is an explanation of the physical forcing mechanism that produced this seabed geomorphology.The real-time oceanographic data system will provide this essential data so that we can explain how and when the seabed is in motion and how the seabed interacts with the beach,either providing sand to the beach or storing it temporarily or permanently offshore.

英语翻译The nearshore seafloor environments may be linked to some degree with the stability and behavior of the barrier-island coastline.Recent sonar images of two small areas on the inner shelf have revealed extensive hardgrounds and complex san
环境也许与某一障碍海岛海岸线的程度与稳定和行为连接.二个小范围的最近生波探侧器图象在内在架子显露了广泛的hardgrounds 和复杂沙子波浪结构表明活跃沉积运输.生波探侧器图象收集了一年单独建议大近海沙子土坎(公里的一些迁移在标度) 可以发生.但是,什么是缺掉是导致这海底地貌学物理强迫的机制的解释.实时海洋学数据系统将提供这根本数据以便我们能解释怎样并且何时海底是在行动并且怎么海底与海滩相处融洽,或提供沙子对海滩或存放它临时地或永久地近海处

nearshore seafloor 环境也许与某一障碍海岛海岸线的程度与稳定和行为连接。二个小范围的最近生波探侧器图象在内在架子显露了广泛的hardgrounds 和复杂沙子波浪结构表明活跃沉积运输。生波探侧器图象收集了一年单独建议大近海沙子土坎(公里的一些迁移在标度) 可以发生。但是, 什么是缺掉是导致这海底地貌学物理强迫的机制的解释。实时海洋学数据系统将提供这根本数据以便我们能解释怎样并且何...

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nearshore seafloor 环境也许与某一障碍海岛海岸线的程度与稳定和行为连接。二个小范围的最近生波探侧器图象在内在架子显露了广泛的hardgrounds 和复杂沙子波浪结构表明活跃沉积运输。生波探侧器图象收集了一年单独建议大近海沙子土坎(公里的一些迁移在标度) 可以发生。但是, 什么是缺掉是导致这海底地貌学物理强迫的机制的解释。实时海洋学数据系统将提供这根本数据以便我们能解释怎样并且何时海底是在行动并且怎么海底与海滩相处融洽, 或提供沙子对海滩或存放它临时地或永久地近海处。

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